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550:342 Technical Series Soils in Construction Soils and Sitework Earthwork: support intended use cut and fill material nature and location of rock Footings and bearing capacity Foundations: structural design Drainage surface drainage Requirements: subsurface drainage susceptibility to erosion dry wells septic systems © Fine Homebuilding

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  • 550:342Technical

    Series

    Soils in Construction

    Soils and Sitework

    Earthwork: support intended use cut and fill material nature and location of rock

    Footings and bearing capacity Foundations: structural design

    Drainage surface drainageRequirements: subsurface drainage

    susceptibility to erosiondry wellsseptic systems

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    Soils in Construction

    Soil Exploration

    Land Use Feasibility: geological maps soil surveysUSGS maps on-site analysis

    Construction Documents: site-specific, detailed informationsoil borings and test pits

    Critical Conditions: organic soils, silt clays, loose siltsfine water-bearing sandhigh water tablerock close to surfaceland fills, dumps, unconsolidated fillsevidence of earth movement

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    Soils in Construction

    Soil Investigation

    Fine Homebuilding

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    Soils in Construction

    Soil Investigation

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    Soils in Construction

    Soil Investigation

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    Soil Characteristics

    Phase Diagrams

    Weight

    Wt = Ww + Ws

    Volume

    Vt = Vv + Vs= Va + Vw + Vs

    From SOIL MECHANICS, College of Engineering, Florida State University

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    Soil Density

    May be referred to as: Bulk Density Unit Weight

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    Water Content

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    Void Ratio

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    Porosity

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    Soils in Construction

    Soil Classification Systems

    United States Department of Agriculture (USDA) Soil Triangle

    American Association of State Highway and Transportation Officials(AASHTO)

    Federal Aviation Administration (FAA)

    Standard Soil Classification System (ASTM D2487)Formerly the Unified Classification System, the most common system used in construction.

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    Standard Soil Classification System ASTM D2487

    Based primarily on those characteristics that indicate how soil willbehave as a construction material.

    Classification procedure includes:

    Sieve (mechanical) Analysis (ASTM D422) Particle Size Distribution Curve Liquid and Plastic Limit

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    Sieve Analysis

    Sieve Analysis

    Soil is passed through a set of sieves with openings of known sizes and then the amount of soil retained on each sieve is weighed.

    Sieve analysis is used to classify coarse soils sands and gravels.

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    Sieve Analysis

    Portland Cement Association

    Soil Fraction Size Range

    Cobble > 3

    GravelCoarse 3 to Fine to No. 4 Sieve

    SandCoarse No. 4 to No. 10Medium No. 10 to No. 40Fine No. 40 to No. 200

    Fines (silt or clay) < No. 200

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    Unified Soil Classification System: Coarse Grained

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    Unified Soil Classification System: Coarse Grained

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    Understanding Sieve Analysis Curves

    GRAVEL

    Above No. 4 Sieve

    SAND

    Between No. 4 Sieve And No. 200 Sieve

    SILT/CLAY

    Below No. 200 Sieve

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    Sieve Analysis Curves: Well Graded Gravel

    Curve 1

    Coarse Fraction: 97%Retained Above Sieve No. 4: 75%

    Curve 2

    Coarse Fraction: 100%Retained Above Sieve No. 4: 46%

    This is not more than 50% of the coarse Fraction, therefore SOIL 2 is a SAND.

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    Definitions

    Well-graded: a coarse grained soil (sand or gravel) with a widerange of particle sizes. Also referred to as:

    Dense graded

    Poorly-graded: a coarse grained soil (sand or gravel) with a limitedrange of particle sizes. Also referred to as:

    Open gradedUniform gradedGap graded

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    Unified Soil Classification System: Coarse Grained

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    Sieve Analysis Curves: Well Graded Sand

    Curve 1

    Coarse Fraction: 97%Retained Above Sieve No. 4: 0%

    Curve 2

    Coarse Fraction: 98%Retained Above Sieve No. 4: 34%

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    Particle Size Distribution

    Uniformity Coefficient Cu (measure of the particle size range)

    Cu = D60/D10Cu < 5: Very Uniform Cu = 5: Medium Uniform Cu > 5: Non-uniform

    Coefficient of Gradation or Curvature Cg [Cc](measure of the shape of the particle size curve)

    Cg = (D30)2/ D60 x D10

    Cg from 1 to 3: well graded

    Where: D10 = diameter of particle size at 10% passingD30 = diameter of particle size at 30% passingD60 = diameter of particle size at 60% passing

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    Sieve Analysis Curves: Well Graded Sand

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    Definitions

    Liquid Limit: the water content, as determined by the standard (LL) liquid limit test (ASTM D423), at which a soil passes

    from a plastic to a liquid state.

    Plastic Limit: the lowest water content, as determined by the (PL) standard plastic limit test (ASTM D424), at which a

    soil remains plastic.

    Plasticity Index: the difference between the liquid limit (LL) and plastic(PI) limit (PL), or the range of water contents over which a

    soil exhibits plastic behavior.

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    Behavior Analysis

    Solid Semi-Solid Plastic Liquid

    SL PL LL

    Increasing water content

    Plasticity Index (PI) = LL PL

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    Sieve Analysis Curves

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    Unified Soil Classification System: Fine Grained

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    Soil Classification

    From SOIL MECHANICS, College of Engineering, Florida State University

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    Frost Penetration

    Ice layers grow from top down.

    Conditions necessary to increase ice thickness:

    Freezing temperature in soil Water table close to frost table Characteristics necessary for rapid capillary action

    Soil heaves equal to ice thickness causing pavementdisplacement

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    Frost Penetration

    Methods to reduce or prevent frost action:

    Use non-frost-susceptible base or sub-base Extend structure below frost line Use cut-off blanket between subgrade and sub-base/base Lower water table

    Thawing creates a super-saturated soil, significantly reducing bearing capacity.This condition often results in pavement failure.

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    Shear Strength

    The stability of a soil and its ability to resist failure under loading is derived from itsshear strength. The shearing strength of a soil is the result of friction between particles and cohesion. Shear strength is not constant, since cohesion varies with water content, rate and duration of loading, confining pressures and other factors.

    Granular Soils have internal friction resistance. have no cohesion. strength increases with increased normal pressure. safe slopes of granular bank do not decrease with increased height.

    Cohesive Soils have cohesive bonding. have no internal friction. strength is the same regardless of normal pressure. safe slopes of cohesive bank becomes flatter as bank height increases, sincestrength does not increase.

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    Shear Strength

    granular soil

    cohesive soil

    heights

    t

    r

    e

    n

    g

    t

    h

    In reality, most soils consist of bothgranular and cohesive components, thus deriving strength from internalfriction and cohesion.

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    Swell and Shrinkage

    Swelling and shrinkage are the result of a build-up and release of water within the soil pore spaces.

    Fine grained soils most susceptible to swelling and shrinking.

    Shrinkage in clay very slow, while rapid in granular soils.

    Shrinkage affects settlement on clay more than on granular soils.

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    Soil Compaction

    From SOIL MECHANICS, College of Engineering, Florida State University

    The degree of compaction of soil is measured by its unit

    weight (or density) and optimum moisture content.

    The process of soil compaction is simply

    expelling the air from the voids or reducing air voids.

    As soil is compacted, soil density is increased.

    Reducing, or squeezing, water from the voids is

    referred to as consolidation, not compaction.

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    Soil Compaction

    In the construction of streets, parking areas, embankments and many other site development projects, it may be necessary to compact soils to increase their density.

    Compaction improves the following characteristics of soils for engineering purposes: Increases Strength Decreases permeability Reduces settlement of foundation Increases slope stability of embankments

    Soil compaction can be achieved either by static or dynamic loading: Smooth-wheel rollers Sheepsfoot rollers Rubber-tired rollers Vibratory Rollers Vibratory Tampers

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    Placing and Compacting Soil

    Placement of Fill Material

    Topsoil should be removed in fill areas

    If area is to support structures (pavements, footings, foundations, etc.), subgrade should be compacted according to engineers specifications, including depth, density and moisture content.

    To minimize settlement, fill should be placed and compacted in layers, referred to as lifts.

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    Placing and Compacting Soil

    Fine Homebuilding

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    Soils in Construction

    Placing and Compacting Soil

    Compaction

    Compaction specifications for structural soils should include density and optimum moisture content.

    Range of optimum moisture content: Sand 8% Silt 15% Clay 15 20%

    Water content should be controlled in making fills Control stormwater runoff. Discharge water away from trenches and excavations. Trenches and excavations should be dewatered.

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    Placing and Compacting Soil

    Compaction Methods

    Rolling is the primary method. Three basic roller types:

    Steel-wheeled: recommended for hard, angularmaterial. Rubber tired: recommended for softer material(sandy soils) and for rolling during final shapingoperations. Sheepsfoot or tamping: recommended for clay.

    Heavy rubber-tired earth moving equipment such asdump trucks assist in compaction during deposition ofsuccessive layer.

    Rammers, tampers and plate vibrators are used to compacttrench excavations, excavations in tight spaces, and againstretaining and foundation walls.

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    Controlled Fill

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    Controlled Fill

    grade stakes

    organic and clay soils

    controlled sand fill

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    Subgrade for Pavement

    Removing poor subgrade soils after pavement failure.

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    Subgrade for Pavement

    Removal of topsoil and preparation of subgrade for asphalt pavement.

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    Subgrade for Pavement

    Final preparation of subgrade. Base and sub-base material to be placed on top of prepared subgrade. Base is opengraded gravel, while sub-base is densegraded gravel.

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    Geotextiles

    Geotextiles apply to a broad range of civil engineering construction, paving, drainage, and other applications.

    Engineered geotextiles perform three basic functions: separation stabilization filtration

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    Geotextiles

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    Geotextiles

    Woven Geotextiles are generally preferred for applications where high strength properties are needed, but where filtration requirements are less critical and planar flow is not a consideration.

    Nonwoven Geotextiles are needle-punched continuous filament engineering fabrics capable of providing planar water flow in addition to their soil stabilization and separation functions. Typical applications include access roads, aggregate drains, asphalt pavement overlays, and erosion control.

    For applications such as roadways, parking lots, loading areas, and construction sites, geotextiles reduce subsoil migration into the aggregate base course, enhancing the long-term performance of the base course while preserving its drainage and structural capacities.Under heavy traffic and construction loads, Woven Geotextiles reduce localized shear failure in weak subsoil conditions.

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    Geotextiles

    Confinement: Maintains base thickness and high friction, thus maintaining design strength of base course.

    Load Distribution: Reduces localized stress by distributing loads over wider area of subgrade.

    Separation: Serves as a barrier between fine grain soils and aggregates. Eliminates the loss of aggregates into subgrade and the pumping of silt and fine grain soils into aggregate.

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    Specifications

    Construction Specifications Institute MasterSpecRelevant Soil Specification Sections:

    2210 Subsurface Investigation2230 Site Clearing (stripping & stockpiling topsoil)2310 Grading2315 Excavation and Fill2340 Soil Stabilization2370 Erosion and Sedimentation Control